Global sedimentary hiatuses are well-documented in ancient pelagic sediment, and include
Paleocene, Eocene-Oligocene boundary, and Miocene hiatuses. Less clear is the extent of …

Hybrid flows comprising both turbidity current and submarine debris flow are a significant
departure from many previous influential models for submarine sediment density flows …

Most of the basins developed in the continental core of SE Asia (Sundaland) evolved since
the Late Cretaceous in a manner that may be correlated to the conditions of the subduction …

This review chiefly examines data on the regionally important Base Miocene Unconformity,
confirming its age and expression in west Sabah, then integrates this with data on the …

Abstract During the Paleogene the Proto-South China Sea was subducted beneath northern
Borneo. Subduction ended with Early Miocene collision of the Dangerous Grounds/Reed …

ABSTRACT The West Baram Line separates NW Borneo's two petroleum systems.
Oligocene sandstone and Lower Miocene carbonate reservoirs of the gas-prone Luconia …

The down‐dip portion of submarine fans comprises terminal lobes that consist of various
gravity flow deposits, including turbidites and debrites. Within lobe complexes, lobe …

Hybrid event beds comprising both clean and mud‐rich sandstone are important
components of many deep‐water systems and reflect the passage of turbulent sediment …

Flutes and tool marks are commonly observed sedimentary structures on the bases of
sandstones in deep‐water successions. These sole structures are universally used as …

Abstract The Borneo Accretionary Orogen (BAO) is located in a central position of SE Asia,
surrounded by the long‐lived westward subduction of the Pacific Plate, northward …